A low-dimensional nonlinear model for the normal velocity (v) and normal vorticity (η) disturbance development in plane Poiseuille flow is studied. The study is restricted to the interactions of a pair of oblique components of the form ei(αx±βz) and the component of the form ei2βz, where α and β are streamwise and spanwise wave numbers, respectively. The disturbances considered are also assumed to be highly elongated in the streamwise direction. Owing to the non-normal properties of the basic equations, the η disturbance is first transiently amplified. Then, if the Reynolds number (R) and the initial disturbance are sufficiently large, the nonlinear interactions lead to a self-sustained process of disturbance amplification at subcritical R. For large R(R≳5000), the threshold disturbance amplitude scales like R−3. The results also strongly indicate that the nonlinear feedback from η to v is crucial for the establishment of the self-sustained process.

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